Ontario Geological Survey
Permanent Link to this Record:
MDI52N04SW00021
Record Name(s) | Craibbe-Fletcher Gold Mines Prospect - 1944, Fletcher Group - 1944 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Developed Prospect Without Reported Reserves or Resources |
Date Created | 1983-Sep-14 |
Date Last Modified | 2022-Sep-27 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Dome
Latitude: 51° 3' 58.47" Longitude: -93° 46' 4.81"
UTM Zone: 15 Easting: 446186.63 Northing: 5657471.99 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04SW
Point Location Description: Iron Formation on est bndy clm KRL 8146
Location Method: Data Compilation
Access Description: Access by a drift on the 2050 foot level of Campbell Mine.
1940: Surface work performed on property. 1944: Craibbe-Fletcher Gold Mines incorporated to acquire property. 1945-47: Sylvanite Gold Mines and Rouyn Gold Mines optioned property. Magnetometer survey completed and approximately 50 holes drilled totalling 10,540 m. 1955: New Dickenson Mines assumed control of Craibbe-Fletcher, performed surface exploration, previous drilling was re-examined, and 6 holes were drilled totalling 1353.59 m. Horizontal drive from the 2050 ft level of Campbell mine extends 1475 feet into the property. 1958-61: 704.86 m of surface drilling, underground work from the 625.25 m level at Campbell consisted of extending a drive 450 m into Craibbe-Fletcher ground and 2507.1 m of underground drilling. 1982-83: Campbell Red Lake Gold Mines buys controlling interest, performs line cutting, surface work.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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63.11 | 52N04SW0086 | 52N04SW0086 |
63.3575 | 52N04NE9929 | 52N04NE9929 |
63.3143 | 52N04NW0001 | 52N04NW0001 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (K R Kettles) - Most of the property is underlain by altered mafic metavolcanic flows. They are comprised mainly of massive basalts with two zones of strongly carbonatized breccia that are thought to be flow top material. A coarser-grained flow unit, locally called the Campbell Diorite , has been recognized on the property. Adjacent to Highway 125 a narrow band of pillowed flows extends across the property. In the northern part of the property, 2 bands of felsic volcanic rocks with associated bands of lean cherty iron formation are known to occur. The general strike in the area is about N70 degs W, and dips vary between 70 degs S to 75 degs S.
Rock Type | Rank | Composition | Texture | Relationship | Mafic massive flow | 1 | Altered Basalt | Massive Flows/Southern | Host |
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Ironstone-unsubdivided | 2 | Lean Cherty Mineralized | Iron Formation-Southern Zone | Host |
Felsic lava flow-unsubdivided | 3 | Silicified | Northern Zone | Host |
Dec 07, 2005 (K R Kettles) - The mafic volcanics are massive basalts with two zones of strongly carbonatized breccia thought to be flow top material.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Pyrrhotite | Economic | Ore | ||||
3 | Sphalerite | Economic | Ore | ||||
4 | Gold | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Carbonate | Economic | Gangue | ||||
3 | Chert | Economic | Gangue | ||||
Carbonate | Alteration | Carbonatization | 1 | Unknown | Disseminated | ||
Silica | Alteration | Silicification | 2 | Unknown | Disseminated |
Dec 07, 2005 (K R Kettles) - Ore grade values of gold occur in two parallel lenses about 30 m apart over a length of over 90 m. The southern zone is contained in mineralized cherty iron formation and silicified and carbonatized mafic volcanic rocks. The northern zone is situated in a run of silicified felsic volcanic rocks. Both zones strike at about N 70 degs W and dip 60 to 70 degs SW. Early drilling gave the following intersections for holes drilled at 30 m intervals (holes listed E to W): SOUTH LENS: DDH44- 0.42 opt Au at 45.75 m;DDH 50- 0.30 opt Au at 117.43 m; DDH43 - 1.24 opt Au at 59.48 m; DDH42 - 0.30 opt Au at 70.15 m; DDH38 - 0.415 opt Au at 79.30 m. NORTH LENS: DDH17 - 0.08 opt Au at 230.28 m; DDH44 - 0.07 opt Au at 79.30 m; DDH43 - 0.64 opt Au at 91.50 m; DDH42 - 0.17 opt Au at 88.45 m.
Dec 07, 2005 (K R Kettles) - The volcanic rocks have been carbonatized and silicified, and the iron formation contains sulphides.
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 90 | 110 | 65 |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 90 | 110 | 65 |
Date: Feb 02, 1997
Geologist: K R Kettles
Notes: N/A
File - Resident Geologist files RL 1928-46 Dome #12
Publication Number: Date:
Author:
Publisher Name:
Location: Red Lake RGP office
Map - Dome Township, Kenora District
Publication Number: M2074 Scale: 1:12,000 Date: 1997
Author: Ferguson S.A.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of Dome Township, District of Kenora
Publication Number: R045 Page: 58-60 Date: 1997
Author: Ferguson S.A.
Publisher Name: Ontario Dept. of Mines
Location:
Part - Geology and mineral deposits of the Red Lake area
Publication Number: ARV49-02 Page: 109 Date: 1998
Author: Horwood H.C.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 208-209 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 428-429 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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